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- W310048675 abstract "The coastal dunes of Aquitaine number more than 1500, and have a total included volume of between 10 and 20 X 109 m3. There are four major types of dunes: parabolic dunes, barchans, round dunes and the foredune. All the dunes were constructed by westerly winds, blowing off the sea. Dating of these dunes is based on paleosols of the Great Dune of Pilat, the highest dune in Europe. The base of this dune is dated at about 3500 years B.P., but most of the dunes were probably formed during the last 2000 years. These dunes obstructed a number of small rivers inducing the development of lakes lie behind them. One small estuary was transformed into a lagoon, the Arcachon lagoon. The sands which built the dunes come from the Atlantic coastal beaches. The present rate of coastal retreat is about 1 to 2 m a year. The coastal erosion rates now observed can be used to estimate the rate of intrusion of sand inland from the coast. Measurements with sand traps and by cartographic comparison give an eastward aeolian flux estimated of between 15 and 30 m3 a year per m length of foredune." @default.
- W310048675 created "2016-06-24" @default.
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- W310048675 date "1991-01-01" @default.
- W310048675 modified "2023-09-26" @default.
- W310048675 title "Coastal erosion and aeolian sand transport on the Aquitaine coast, France" @default.
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- W310048675 doi "https://doi.org/10.1007/978-3-7091-6703-8_11" @default.
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